Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina
Granitoid and volcanic rocks of the Cordillera Neuquina between 38°45′ and 39°30′ south latitude have been metamorphosed under zeolite, prehnite-pumpellyite, and transitional greenschist facies conditions. This low-grade metamorphism is related to the circulation of hydrothermal solutions associated...
Guardado en:
Autores principales: | , |
---|---|
Formato: | JOUR |
Materias: | |
Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_08959811_v3_n4_p247_VattuonedePonti |
Aporte de: |
id |
todo:paper_08959811_v3_n4_p247_VattuonedePonti |
---|---|
record_format |
dspace |
spelling |
todo:paper_08959811_v3_n4_p247_VattuonedePonti2023-10-03T15:43:06Z Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina Vattuone de Ponti, M.E. Latorre, C.O. granitoid greenschist facies metamorphism prehnite pumpellyite volcanic rock zeolite Argentina, Cordillera Neuquina Granitoid and volcanic rocks of the Cordillera Neuquina between 38°45′ and 39°30′ south latitude have been metamorphosed under zeolite, prehnite-pumpellyite, and transitional greenschist facies conditions. This low-grade metamorphism is related to the circulation of hydrothermal solutions associated with Tertiary(?) subvolcanic bodies and/or shallow intrusives through a pre-existing fracture system. Three progressive metamorphic zones have been established, with temperatures ranging from 100° to 300°C and pressures less than 4 kb. The pressures are similar to those estimated for metamorphic rocks at Taringatura, New Zealand, and in the Tanzawa Mountains of Japan. The mineral assemblages are influenced by host-rock composition. In the granitoids, the sequence is: Zone I - heulandite, stilbite, K-feldspar, albite, quartz, calcite; Zone II - chlorite, prehnite, pumpellyite, albite, K-feldspar, titanite, quartz; and Zone III - chlorite, pistacite, piedmontite, titanite, actinolite, K-feldspar, albite, quartz, calcite. In the basalts, the sequence is: Zone I - heulandite, stilbite, calcite; Zone II - analcime, thomsonite, laumontite, natrolite, celadonite, albite; and Zone III - chlorite, pistacite, actinolite, pumpellyite, laumontite, albite, quartz. In the andesites, the sequence is: Zone I - stilbite, calcite, quartz; Zone II - pumpellyite, chlorite, titanite, celadonite, albite, quartz, calcite; and in Zone III - pistacite, quartz, chlorite, albite. Pyrite, chalcopyrite, arsenopyrite, and copper are always found in association with quartz and epidote in Zone III. © 1991. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_08959811_v3_n4_p247_VattuonedePonti |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
granitoid greenschist facies metamorphism prehnite pumpellyite volcanic rock zeolite Argentina, Cordillera Neuquina |
spellingShingle |
granitoid greenschist facies metamorphism prehnite pumpellyite volcanic rock zeolite Argentina, Cordillera Neuquina Vattuone de Ponti, M.E. Latorre, C.O. Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina |
topic_facet |
granitoid greenschist facies metamorphism prehnite pumpellyite volcanic rock zeolite Argentina, Cordillera Neuquina |
description |
Granitoid and volcanic rocks of the Cordillera Neuquina between 38°45′ and 39°30′ south latitude have been metamorphosed under zeolite, prehnite-pumpellyite, and transitional greenschist facies conditions. This low-grade metamorphism is related to the circulation of hydrothermal solutions associated with Tertiary(?) subvolcanic bodies and/or shallow intrusives through a pre-existing fracture system. Three progressive metamorphic zones have been established, with temperatures ranging from 100° to 300°C and pressures less than 4 kb. The pressures are similar to those estimated for metamorphic rocks at Taringatura, New Zealand, and in the Tanzawa Mountains of Japan. The mineral assemblages are influenced by host-rock composition. In the granitoids, the sequence is: Zone I - heulandite, stilbite, K-feldspar, albite, quartz, calcite; Zone II - chlorite, prehnite, pumpellyite, albite, K-feldspar, titanite, quartz; and Zone III - chlorite, pistacite, piedmontite, titanite, actinolite, K-feldspar, albite, quartz, calcite. In the basalts, the sequence is: Zone I - heulandite, stilbite, calcite; Zone II - analcime, thomsonite, laumontite, natrolite, celadonite, albite; and Zone III - chlorite, pistacite, actinolite, pumpellyite, laumontite, albite, quartz. In the andesites, the sequence is: Zone I - stilbite, calcite, quartz; Zone II - pumpellyite, chlorite, titanite, celadonite, albite, quartz, calcite; and in Zone III - pistacite, quartz, chlorite, albite. Pyrite, chalcopyrite, arsenopyrite, and copper are always found in association with quartz and epidote in Zone III. © 1991. |
format |
JOUR |
author |
Vattuone de Ponti, M.E. Latorre, C.O. |
author_facet |
Vattuone de Ponti, M.E. Latorre, C.O. |
author_sort |
Vattuone de Ponti, M.E. |
title |
Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina |
title_short |
Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina |
title_full |
Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina |
title_fullStr |
Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina |
title_full_unstemmed |
Low-grade metamorphism in granitoids and volcanic rocks, Cordillera Neuquina, Argentina |
title_sort |
low-grade metamorphism in granitoids and volcanic rocks, cordillera neuquina, argentina |
url |
http://hdl.handle.net/20.500.12110/paper_08959811_v3_n4_p247_VattuonedePonti |
work_keys_str_mv |
AT vattuonedepontime lowgrademetamorphismingranitoidsandvolcanicrockscordilleraneuquinaargentina AT latorreco lowgrademetamorphismingranitoidsandvolcanicrockscordilleraneuquinaargentina |
_version_ |
1782024120926470144 |